Mg/Ca ratio in stalactite indicates drought at time of extinction of Homo floresiensis ("Hobbits")

alanw

Well-known member


In optimal karst settings, speleothem Mg/Ca serves as an independent indicator of past changes in local monsoon rainfall. Accumulating evidence shows that prior calcite precipitation (PCP) in karst void spaces, where CO2 degassing occurs, can increase Mg/Ca in cave dripwaters due to preferential exclusion of Mg2+ during calcite formation. Reduced rainfall and karst infiltration rates create conditions favouring PCP, resulting in higher Mg/Ca in the speleothem ‘downstream’. In principle, tandem measurements of Mg/Ca and δ18O in speleothems can be used to infer rainfall seasonality.
 
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